The Weierbach experimental catchment (0.45 km2) is the most instrumented and studied sub-catchment in the Alzette River basin in Luxembourg. Within the last decade, it has matured towards an interdisciplinary critical zone observatory focusing on a better understanding of hydrological and hydro-geochemical processes. Since 2009, the Weierbach has been extensively equipped for continuously monitoring water fluxes and physico-chemical parameters within different compartments of the critical zone. Additionally, these compartments are sampled fortnightly at several locations to analyze d18O and d2H isotopic composition of water including rainfall, throughfall, soil water, groundwater and streamwater. This link provide the entire database acquir...
Isotopes and related data associated with water tracing with environmental DNA in a high-Alpine catc...
In mountainous headwater catchments, with their high variability of hydrological processes and catch...
The water composition of the river Adige displays a Ca–HCO3 hydrochemical facies, mainly due to rock...
The Weierbach experimental catchment (0.45 km2) is the most instrumented and studied sub-catchment i...
ACKNOWLEDGEMENTS The authors are grateful to all colleagues involved in the sample collection and in...
The objective of my Master thesis is to investigate how hydrochemical as well as isotopic tracers ca...
International audienceThe streamflow components were determined in a small catchment located in East...
The stable isotopes of oxygen and hydrogen, 18O and 2H, provide information on water flow pathways a...
A dual stable water isotope (d2H and d18O) study was conducted in the developed (managed) landscape ...
Data collected in the Otemma forefield in Switzerland (45°56’03”N,7°24’42”) from July 2019 to Octobe...
The Wüstebach catchment belongs to the German TERENO (Terrestrial Environmental Observatories) netwo...
International audienceIn order to characterize the chemical composition and the age of the water cir...
Database gathering 2862 water samples from the Vallon de Nant (Westerm Swiss Alps) analyzed for stab...
Over the past decades, interpretation of changes in stable isotope signatures of catchment waters ha...
Two groundwater bodies, Grazer Feld and Leibnitzer Feld, with surface areas of 166 and 103 km2 respe...
Isotopes and related data associated with water tracing with environmental DNA in a high-Alpine catc...
In mountainous headwater catchments, with their high variability of hydrological processes and catch...
The water composition of the river Adige displays a Ca–HCO3 hydrochemical facies, mainly due to rock...
The Weierbach experimental catchment (0.45 km2) is the most instrumented and studied sub-catchment i...
ACKNOWLEDGEMENTS The authors are grateful to all colleagues involved in the sample collection and in...
The objective of my Master thesis is to investigate how hydrochemical as well as isotopic tracers ca...
International audienceThe streamflow components were determined in a small catchment located in East...
The stable isotopes of oxygen and hydrogen, 18O and 2H, provide information on water flow pathways a...
A dual stable water isotope (d2H and d18O) study was conducted in the developed (managed) landscape ...
Data collected in the Otemma forefield in Switzerland (45°56’03”N,7°24’42”) from July 2019 to Octobe...
The Wüstebach catchment belongs to the German TERENO (Terrestrial Environmental Observatories) netwo...
International audienceIn order to characterize the chemical composition and the age of the water cir...
Database gathering 2862 water samples from the Vallon de Nant (Westerm Swiss Alps) analyzed for stab...
Over the past decades, interpretation of changes in stable isotope signatures of catchment waters ha...
Two groundwater bodies, Grazer Feld and Leibnitzer Feld, with surface areas of 166 and 103 km2 respe...
Isotopes and related data associated with water tracing with environmental DNA in a high-Alpine catc...
In mountainous headwater catchments, with their high variability of hydrological processes and catch...
The water composition of the river Adige displays a Ca–HCO3 hydrochemical facies, mainly due to rock...